Petrogenesis for the Chiang Dao Permian high-iron basalt and its implication on the Paleotethyan Ocean in NW Thailand

Yuzhi Zhang; Yuejun Wang; Boontarika Srithai; Burapha Phajuy

doi:10.1007/s12583-015-0646-4

Volume 27 Issue 3

Jun 2016

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Journal of Earth Science > 2016 > 27(3): 425-434.

Yuzhi Zhang, Yuejun Wang, Boontarika Srithai, Burapha Phajuy. Petrogenesis for the Chiang Dao Permian high-iron basalt and its implication on the Paleotethyan Ocean in NW Thailand. Journal of Earth Science, 2016, 27(3): 425-434. doi: 10.1007/s12583-015-0646-4

Citation:

Yuzhi Zhang, Yuejun Wang, Boontarika Srithai, Burapha Phajuy. Petrogenesis for the Chiang Dao Permian high-iron basalt and its implication on the Paleotethyan Ocean in NW Thailand. Journal of Earth Science, 2016, 27(3): 425-434. doi: 10.1007/s12583-015-0646-4

Citation:

Yuzhi Zhang, Yuejun Wang, Boontarika Srithai, Burapha Phajuy. Petrogenesis for the Chiang Dao Permian high-iron basalt and its implication on the Paleotethyan Ocean in NW Thailand. Journal of Earth Science, 2016, 27(3): 425-434. doi: 10.1007/s12583-015-0646-4

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Petrogenesis for the Chiang Dao Permian high-iron basalt and its implication on the Paleotethyan Ocean in NW Thailand

doi: 10.1007/s12583-015-0646-4

1.
School of Earth Science and Geological Engineering, Sun Yat-sen University, Guangzhou, 510275, China
2.
CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, 100101, China
3.
Department of Geological Sciences, Faculty of Science, Chiang Mai University, Chiang Mai, 50200, Thailand

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Corresponding author: Yuejun Wang, wangyuejun@mail.sysu.edu.cn
Received Date: 07 Jun 2015
Accepted Date: 18 Oct 2015
Publish Date: 10 Jun 2016

Abstract

Abstract

The Changning-Menglian suture in SW Yunnan has been accepted as the Paleotethyan main ocean. However, it has been a matter of debate as to its southerly extension in NW Thailand (the Chiang Mai-Chiang Rai vs. Nan-Uttaradit zone). Our field investigation identified the high-iron basaltic rocks in the Chiang Dao Permian standard profile in NW Thailand. The high-iron rocks provide crucial records for understanding the controversy on the location of Paleotethyan main ocean in NW Thailand. The Early Permian high-iron samples show extremely high FeOt (20.96 wt.%–25.56 wt.%) and TiO₂ (6.07 wt.%–6.34 wt.%) and low SiO₂ (38.54 wt.%–43.46 wt.%) and MgO (1.61 wt.%–2.40 wt.%) contents. Such characteristics are similar to those of the Fenner differentiation trend rarely observed in the natural system, distinct from those of the "normal" Bowen trend. Their chondritenormalized REE and primitive mantle-normalized patterns are generally similar to those of typical OIB. The initial ⁸⁷Sr/⁸⁶Sr ratios and εNd(t) values range from 0.704 677 to 0.705 103 and 3.16 to 3.48, respectively, falling near the field of typical OIB (oceanic-island basalt). These data synthetically suggest that the Chiang Dao high-iron rocks are the products of high-degree partial melting of peridotite with Fe-rich eclogitic blobs/streaks in response to a seamount setting. In comparison with the Permian tectonic setting in SW Yunnan and NW Thailand, it is inferred that the Paleotethyan Ocean was located between the Shan-Thai terrane of Sibumasu and Sukhothai arc along the Inthanon zone of the Chiang Mai-Chiang Rai rather than Nan-Uttaradit zones.
- high-iron rock,
- Fenner differentiation trend,
- Chiang Dao OIB-like basalt,
- Paleotethyan Ocean,
- seamount setting

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